6
G. Aiello et al.
100 m nw
se
110 m
120 m
8010 subbottom Chirp line
130 m
. . .,~ ... "
110 m
120 m
130 m
Fig.6. Subbottom chirp profile showing creep in Holocene sediments off the Sarno river mouth. Creep movements involve the
sediments above a surface of separation, interpreted as a maximum flooding surface
SE
..... 200
300
400
500
maac (1wI)
coa&tIll sand barB
1 km
ovem.nk deposita with
channel levee oomple_
i
(IOIIt-1ff! prograding wadg
---'-~-(Midd18 PleIStocerie)
UNESPK8
NW
Fig.7. Line drawing of the Sparker line SP8 showing the canyoning engraving down to the Middle-Late Pleistocene prograding
units. Note the occurrence of a peculiar seismic unit interpreted as overbank deposits with channel-Iev~e complexes. A top of
Mesozoic carbonatic acoustic basement; B top of Miocene flysch deposits; C erosional truncation involving the Early-Middle
Pleistocene prograding wedge; D erosional truncation involving the Middle Pleistocene prograding wedge